4.6 Article

Impact of urban canopy models and external parameters on the modelled urban energy balance in a tropical city

期刊

出版社

WILEY
DOI: 10.1002/qj.3028

关键词

urban canopy models; surface energy balance; tropical residential neighbourhood; water vapor opacity; surface interception distribution; local climate zones

资金

  1. Flemish regional government through a FWO (Fund for Scientific Research) post-doctoral position
  2. FWO mobility grant
  3. Hercules foundation
  4. Flemish Government (EWI)
  5. Academy of Finland [138328, 1127756, 281255, 263149]
  6. National Science Foundation (NSF)
  7. Belgian Science Policy Office through its Science for a Sustainable Development Programme [SD/CS/041/MACCBET, BR/143/A2/CORDEX.be]
  8. National Research Foundation Singapore through the Singapore MIT Alliance for Research and Technology's CENSAM research program
  9. National University of Singapore [R-109-000-091-112]
  10. Met Office/Newton Fund CSSP-China
  11. NERC [NE/L008971/1] Funding Source: UKRI
  12. Natural Environment Research Council [NE/L008971/1] Funding Source: researchfish
  13. Academy of Finland (AKA) [263149, 263149] Funding Source: Academy of Finland (AKA)

向作者/读者索取更多资源

To date, existing urban land surface models (ULSMs) have been mostly evaluated and optimized for mid-and high-latitude cities. For the first time, we provide a comparative evaluation of four ULSMs for a tropical residential neighbourhood in Singapore using directly measured energy balance components. The simulations are performed offline, for an 11 month period, using the bulk scheme TERRA URB and three models of intermediate complexity (CLM, SURFEX and SUEWS). In addition, information from three different parameter lists are used to quantify the impact (interaction) of (between) external parameter settings and model formulations on the modelled urban energy balance components. Encouragingly, overall results indicate good model performance for most energy balance components and align well with previous findings for midlatitude regions, suggesting the transferability of these models to (sub) tropical regions. Similar to results from midlatitude regions, the outgoing long-wave radiation and latent heat flux remain the most problematic fluxes. In addition, the various combinations of models and different parameter values suggest that error statistics tend to be dominated more by the choice of the latter than the choice of model. Finally, our intercomparison framework enabled the attribution of common deficiencies in the different model approaches found previously in midlatitude regions: the simple representation of water intercepted by impervious surfaces leading to a positive bias in the latent heat flux directly after a precipitation event; and the positive bias in modelled outgoing long-wave radiation that is partly due to neglecting the radiative interactions of water vapour between the surface and the tower sensor. These findings suggest that future developments in urban climate research should continue the integration of more physically based processes in urban canopy models, ensure the consistency between the observed and modelled atmospheric properties and focus on the correct representation of urban morphology, water storage and thermal and radiative characteristics.

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